Crystallographic analysis of rock grain orientation at meso- and microscale levels

Abstract

This paper studies the results of electron backscatter diffraction analysis of naturally deformed polycrystalline olivine. It also defines the dependence of lattice-preferred orientations of grains on their microstructural position and size. The authors detect the basic mechanisms, consequence and thermal dynamic modes of deformation. They also show that the development of a polycrystalline structure is determined by the following consecutive activation of sliding systems (010)[100] → {0kl}[100] → (100)[010] → {100}[001] → {110}[001], when dislocation sliding and diffusion creep change under the temperature decrease from 1000°C to 650°C.

Original language	English
Title of host publication	AIP Conference Proceedings
Publisher	American Institute of Physics Inc.
Pages	323-326
Number of pages	4
Volume	1623
ISBN (Print)	9780735412606
DOIs	https://doi.org/10.1063/1.4898947
Publication status	Published - 2014
Event	International Conference on Physical Mesomechanics of Multilevel Systems 2014 - Tomsk, Russian Federation Duration: 3 Sep 2014 → 5 Sep 2014

Other

Other	International Conference on Physical Mesomechanics of Multilevel Systems 2014
Country	Russian Federation
City	Tomsk
Period	3.9.14 → 5.9.14

Keywords

EBSD
Lattice-preferred orientation
Olivine
Plastic deformation

ASJC Scopus subject areas

Physics and Astronomy(all)

Access to Document

10.1063/1.4898947

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Cite this

Kulkov, AS, Chernishov, AI, Lychagin, DV, Tishin, PA & Kulkov, SN 2014, Crystallographic analysis of rock grain orientation at meso- and microscale levels. in AIP Conference Proceedings. vol. 1623, American Institute of Physics Inc., pp. 323-326, International Conference on Physical Mesomechanics of Multilevel Systems 2014, Tomsk, Russian Federation, 3.9.14. https://doi.org/10.1063/1.4898947

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abstract = "This paper studies the results of electron backscatter diffraction analysis of naturally deformed polycrystalline olivine. It also defines the dependence of lattice-preferred orientations of grains on their microstructural position and size. The authors detect the basic mechanisms, consequence and thermal dynamic modes of deformation. They also show that the development of a polycrystalline structure is determined by the following consecutive activation of sliding systems (010)[100] → {0kl}[100] → (100)[010] → {100}[001] → {110}[001], when dislocation sliding and diffusion creep change under the temperature decrease from 1000°C to 650°C.",

keywords = "EBSD, Lattice-preferred orientation, Olivine, Plastic deformation",

author = "Kulkov, {A. S.} and Chernishov, {A. I.} and Lychagin, {D. V.} and Tishin, {P. A.} and Kulkov, {S. N.}",

year = "2014",

doi = "10.1063/1.4898947",

language = "English",

isbn = "9780735412606",

volume = "1623",

pages = "323--326",

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AU - Kulkov, A. S.

AU - Chernishov, A. I.

AU - Lychagin, D. V.

AU - Tishin, P. A.

AU - Kulkov, S. N.

PY - 2014

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N2 - This paper studies the results of electron backscatter diffraction analysis of naturally deformed polycrystalline olivine. It also defines the dependence of lattice-preferred orientations of grains on their microstructural position and size. The authors detect the basic mechanisms, consequence and thermal dynamic modes of deformation. They also show that the development of a polycrystalline structure is determined by the following consecutive activation of sliding systems (010)[100] → {0kl}[100] → (100)[010] → {100}[001] → {110}[001], when dislocation sliding and diffusion creep change under the temperature decrease from 1000°C to 650°C.

AB - This paper studies the results of electron backscatter diffraction analysis of naturally deformed polycrystalline olivine. It also defines the dependence of lattice-preferred orientations of grains on their microstructural position and size. The authors detect the basic mechanisms, consequence and thermal dynamic modes of deformation. They also show that the development of a polycrystalline structure is determined by the following consecutive activation of sliding systems (010)[100] → {0kl}[100] → (100)[010] → {100}[001] → {110}[001], when dislocation sliding and diffusion creep change under the temperature decrease from 1000°C to 650°C.

KW - EBSD

KW - Lattice-preferred orientation

KW - Olivine

KW - Plastic deformation

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